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The atmosphere is heated from the bottom by solar radiation and cooled from the top by infrared radiation to space. Mechanical energy is produced when heat is carried upward by convection. The Atmospheric Vortex Engine (AVE) is a process for capturing the energy produced when heat is carried upward by convection in the atmosphere.
The AVE uses a tornado-like vortex to concentrate the mechanical energy produced during upward heat convection where it can be captured. A vortex engine consists of a cylindrical wall open at the top and with tangential air entries or deflectors around its base. Heating the air within the wall using a temporary heat source such as steam starts the vortex. The heat required to sustain the vortex once established can be the natural heat content of the warm humid air or can be provided in cooling towers located outside of the cylindrical wall and upstream of the deflectors. The continuous heat source for the peripheral heat exchangers can be waste industrial heat or warm seawater. The intensity of the vortex is regulated by restricting the flow of air with dampers located upstream of the deflectors. The vortex can be stopped by restricting the airflow to deflectors with direct orientation and if necessary opening the airflow to deflectors with reverse orientation.
The electrical energy is produced in turbo-expanders located upstream of the tangential entries. The pressure at the base of the vortex is less than ambient pressure because the density of the rising air is less than the density of the ambient air at the same level. The outlet pressure of the turbo-expanders is sub-atmospheric because they exhaust in the vortex.
The cylindrical wall could have a diameter of 200 m and a height of 100 m; the vortex could be 50 m in diameter at its base and extend up to the tropopause. An AVE could generate 50 to 500 MW of electrical power.
Thermodynamic Basis
The Atmospheric Vortex Engine has the same thermodynamic basis as the solar chimney. The physical tube of the solar chimney is replaced by centrifugal force in the vortex and the atmospheric boundary layer acts as the solar collector. The AVE needs neither the collector nor the high chimney. The efficiency of the solar chimney is proportional to its height which is limited by practical considerations, but a vortex can extend much higher than a physical chimney.
The average upward convective heat flux at the bottom atmosphere is 150 W/m2, one sixth of this heat could be converted to work while it is carried upward by convection. The heat to work conversion efficiency of the atmosphere is approximately 15% because the heat is received at an average temperature of 15 °C and given up at an average temperature of minus 15 °C. The average work produced in the atmosphere is therefore 25 W/m2. The total mechanical energy produced in the atmosphere is 12000 TW (25 W/m2 x 510 x 10E12 m2) whereas the total work produced by humans is 2 TW. The mechanical energy produced in a single large hurricane can exceed all the energy produced by humans in a whole year.
The thermodynamic basis of the AVE is consistent with currently accepted understanding of how energy is produced in the atmosphere. Atmospheric scientists call the mechanical energy produced when a unit mass of air is raised reversibly from the bottom to the top of the troposphere Convective Available Potential Energy (CAPE). CAPE during periods of insolation or active convection is typically 1500 J/kg which is equal to the mechanical energy produced by lowering a kilogram of water 150 m. The vortex would transfer the mechanical energy down to the Earth's surface where it would be captured.
The existence of tornadoes proves that low intensity solar radiation can produce concentrated mechanical energy. It should be possible to control a naturally occurring process. Controlling where mechanical energy is produced in the atmosphere offers the possibility of harnessing solar energy without having to use solar collectors.
Process Potential
The process could provide large quantity of renewable energy, could alleviate global warming, and could contribute to meeting the requirements of the Kyoto protocol. The AVE has the potential of providing precipitation as well as energy. There is reluctance to attempt to reproduce a phenomenon as destructive as a tornado, but controlled tornadoes could reduce hazards by relieving instability rather than create hazards. A small tornado firmly anchored over a strongly built station need not be a hazard.
The AVE could increase the power output of a thermal power plant by 30% by converting 20% of its waste heat to work. The power increase results from reducing the temperature of the cold sink from the temperature at the bottom of the atmosphere (15 °C) to the temperature at which the atmosphere radiates heat to space (-15 °C).
The process could be adapted for use with all existing thermal power plants, whether they are coal fired, natural gas or nuclear. The main requirement for the AVE is a steady supply of low-grade heat. The temperature of the saturated air coming out of power plant cooling towers is higher than that of the warm humid air responsible for the energy of tornadoes and hurricanes.
The process could be developed with relatively little engineering effort. The technology is similar to that of cooling towers and turbine-generators. The upward heat convection process responsible for producing energy in the AVE is the process responsible for producing the circulation in natural draft cooling towers and in natural circulation boilers. Engineers with experience in the power industry would be good candidate for developing the process.
Electrical utilities are invited to consider participating in the development and commercialization of the AVE. The unit cost of electrical energy produced with an AVE could be less than half the cost of the next most economical alternative. Additional electrical energy would be produced without additional fuel. The process is protected by patent applications and could become an important source of electrical energy.
Initial development work would concentrate on producing stable vortices. Under favorable conditions, it should produce a steam assisted vortex with a station 10 m in diameter and a self-sustaining vortex with a station 30 m in diameter. Learning to control large vortices under all conditions will be an engineering challenge. Developing the process will require determination, engineering resources and cooperation between engineers and atmospheric scientists. There will be difficulties to overcome, but they should be no greater than in other large technical enterprises.
Additional Information
In December 2004, a detailed description of the AVE including drawings and thermodynamic calculations was published as a White Paper in Energy Central's Knowledge Center.
On September 29 2005 the Economist had an article on the AVE which resulted in a lot of media attention: http://www.economist.com/science/displayStory.cfm?story_id=4455446
There is much more information including: drawings, presentations, and technical publications on the AVE web site: http://vortexengine.ca
For information on purchasing reprints of this article, contact Tim Tobeck ttobeck@energycentral.com. Copyright 2010 CyberTech, Inc.
Interesting article and concept. The scientific analysis in the papers at http://www.vortex.com is also impressive. Particularly notable is your explanation of the missing 20 to 30 w/sq m in the climate models, if I understood your paper at http://vortexengine.ca/M25/M25_ARTICLE.htm
Kudos.
Jerry Toman 1.30.06
Well folks, here it is--the opportunity of a lifetime to go down in history as the "hero" who developed the key technology to stop runaway global warming while becoming filthy rich in the process. Not the type of opportunity that comes around every day, month, or year. This one has the potential ta make more money than Google--far more.
Now that I have your attention, let's consider the facts. We know that the light energy from the sun that is not reflected by clouds or snow is absorbed by the oceans or the surface of the earth. The heat generated there is transferred to the lower levels of the atmosphere by conduction and convection. At night (day too), the excess heat is reradiated at longer wave lengths back into outer space. However, greenhouse gases reabsorb some of this, mostly in the lower troposphere. At the top of the troposphere, certain gases, including CO2 reradiate heat more efficiently to outer space, making this altitude colder than would be anticipated based on the adiabatic temperature lapse.
The bottom line is that since the troposphere is heated from below, cooled from above, and "hot air" is less dense than cold air, and tends to rise, the troposphere is, energetically speaking, "upside-down". Another way of looking at it is to say that it is "full of potential energy". One measure of the energy content at a particlular location at a particular time is the CAPE, described in the article.
Well, you ask, why doesn't the troposphere simply "right itself" by flipping over?
The answer is that sometimes it does. However, that is usually not necessary, since the excess heat is "slowly" transported upward during the day by small-scale updrafts and downdrafts and surface winds that impinge on mountain ranges to provide larger-scale turbulence. But the only mechanism that it has to accomplish a "wholesale" overturning from which we can extract work, is through the formation of a "vortex", the common forms of which are tornados and hurricanes. These form to relieve the "excess stress" built up either during the day in the case of tornados, or during the "summer season" in the case of hurricanes.
Now potential energy in the atmosphere is insufficient, by itself, to create a vortex. Rotation of surface winds is also required. Due to particular local wind patters, rotation is achieved in "tornado alley" in the spring. Also, rotation is induced near the equator by Coriolis forces in large-scale air masses, leading the the formation of hurricanes.
The engineering challenge, in my opinion, to developing this technology is to efficiently create enough rotational momentum to the surface air coming into the vortex, by building curved walls, so that it overcomes both friction and "local minima" in the CAPE that may occur at certain altitudes. Adding waste heat energy from existing power plants or warm sea water (Sea of Cortez?) allows the process to continue through the night and is frosting on the cake.
Let's look at additional benefits of the technology: 1) No more coal-fired power plants with the mess of mountain-top removal, mine disasters, mercury pollution, and GW threat. IMO, clean coal is just a ruse to allow building of the plant--CO2 will never be secuestered due to the cost and lack of use or convenient disposal site for the CO2. 2) The efficiency of existing plants can be increased by up to 30% by rejecting waste heat at the level of the tropopause instead of the surface of the earth where it does most harm. 3) Stack gases could efficiently be dispersed to the top of the troposphere while adding energy to the vortex. At the top, any aerosols contained would contribute to "global dimming" a short-term counter to GW. 4) Plants would be relatively smaller than todays central power stations, allowing them to be "distributed" reducing transmission costs. 5) The cheap power could be used to mitigate water shortages in dry areas, either through pumping or desalination, or, in some cases simply causing rain to occur and be collected. 7) Natural gas could be saved by using heat pumps for space heating from the electricity generated. 8) It could be used as a specific tool to cool a location to stop outgassing of the potent GHG, methane, from the tundra. There are others too numerous to name here.
The truth of the matter is that this technology has too much potential "not" to be developed and it will happen sooner or later. The only question is, by whom, and whether it will be soon enough to make a real difference in GW, and before more money is thrown down the pit of more mine activity, coal plants or nuclear energy. If you "nuke lovers" think that a plant can be build for the same cost as thirty years ago, think again. You would have to spend that much on the exchangers alone nowadays.
Isn't it time we complied with rule no. 1 of holes, which is when your getting in too deep, STOP DIGGING. So who's it going to be? A north-american company? What ab
Jerry Toman 1.30.06
What about GE, a slam-dunk with your resources and wind-turbine technology? Or is your "ecoimagination" strictly limited to your PR department. (It takes real imagination to put African elephants and chimps together with Brazilian Macaws in the same location. I didn't know either one even "liked" rain forests that much).
What about the "Oil Companies", or are you still drooling about the potential riches of "buying back stock" and charging people through the nose, instead of finding real energy solutions? Ah, never mind, I think I know the answer. Maybe an independent? Anadarko, or do you think it's even riskier than your "deep water" plan amongst cat-5 hurricanes.
Well, I think if it's going to be done, it won't be here in NA. How about Europe--tired of depending on Russia for your "energy fix". Get used to it and better start polishing up your shuffle. India, China, Brazil--your climates are perfect for this technology and your needs are great. Whaddya say? Are you all going to leave the development task up to a guy in Utah with a business degree, and no budget working with telephone poles? Shame on you.
Why don't we all get together and make this a reality ASAP.
John Robertson 1.31.06
Interesting idea - but the efficiency does not look right. If the average temperature 'in' is 15 C and 'out' is -15 C that corresponds to 288 K and 258 K respectively. In turn that equates to a Carnot efficiency of 10% - not 15 % nor 1/6th. No engine achieves full Carnot efficiency so the efficiency of your machine will be some single figure percent. However, if it works as stated it would still yield a lot of electrical energy.
Best wishes from Oz,
John Robertson
Louis Michaud 2.2.06
Response to John Robertson. You are correct. The average temperature at the bottom of the atmosphere is 15 °C, however, the average temperature at which heat is received by the atmosphere is 25 °C because most of the heat is received in low latitude where the temperature is warmer than average. The statement that 15% of the heat received is converted to work remains valid.
My (1996) paper “Heat to Work Conversion during Upward Heat Convection – Part II” used heat source and sink temperatures of 290 K and 250K. My (2005) AGU presentation “Unrestrained Expansion – a Source of Entropy” used heat source and heat sink temperatures of 288 K and 255 K which is the consensus in the cited recent publications.
The troposphere is cooled by infrared radiation to space at an average rate of 1.5 °C/day. The heat to work conversion efficiency for heat transported from sea level to the 1000 m level is approximately 2%. The heat to work conversion efficiency for heat transported from sea level to the 20000 m level is approximately 30%. The calculations in Table 1 of the “Atmospheric Vortex Engine” technical description show that, for heat carried to the top of the troposphere, the incremental work produced is around 28% of the incremental heat received irrespective of whether the heat is received as sensible or latent heat. Capturing half of the work produced when heat is transported to the top of the troposphere would be sufficient to achieve an overall efficiency of 15%.
Buoyant air tends to rises up to its level of neutral equilibrium. At its final level, the lifted air in not significantly warmer than the ambient air. The warming results from the compression of the underlying air. Raising a 1 kPa layer from the bottom of the atmosphere (100 kPa level) to the 20 kPa level increases the temperature of the air the air originally at the 20 kPa level 4 time more than the temperature of the air at the 80 kPa level because the temperature increase is proportional to the pressure ratio (20 to 21 versus 80 to 81). As a result high updrafts warm the upper troposphere more than the lower troposphere. Deep updrafts increase the temperature of the upper troposphere; shallow updrafts, which are more common than deep updrafts, heat the lower troposphere. See manuscript: “Subsidence required to replace heat loss by infrared radiation to space with work of compression”.
Natural updrafts tend to be shallow because they lose their buoyancy as they are diluted by ambient air. When air rises in a vortex, centrifugal force prevents dilution and therefore the level of neutral buoyancy is higher. The AVE is mainly concerned with the efficiency of deep updrafts since centrifugal force prevents dilution and therefore the updrafts remain buoyant up to the higher level.
arif arif 7.15.09
I think the biggest challenge is the high speed horizontal wind which would decrease its height and decrease power output kW.
arif arif 7.15.09
The efficiency is not a big problem because fuel is free.Why don't this concept be used with water rather air.In tropical coastal areas, roughly between the Tropic of Capricorn and the Tropic of Cancer,the temperature difference between the warmer, top layer of the ocean and the colder, deep ocean water is about 20°C (36°F).the density of water is 700 times greater than air so do the power output kW.